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U-th dating of striated fault planes

Online Publications learn more. To view the site as it was intended, please turn it on and reload the page. Perkins Research Conference. The finalists and their research topics are:.
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U-Th dating of striated fault planes

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Professor Gideon Rosenbaum - UQ Researchers

Gideon Rosenbaum's research interests are in the fields of structural geology and tectonics. He is particularly interested in the geodynamics of convergent plate margins. Tectonics, 38 5 TC, Journal Article: A trapdoor mechanism for slab tearing and melt generation in the northern Andes. A trapdoor mechanism for slab tearing and melt generation in the northern Andes. Geology, 47 1 , Journal Article: Devonian crustal stretching in the northern Tasmanides Australia and implications for oroclinal bending.
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Geology ;; 40 7 : — Direct dating of brittle fault activity is of fundamental importance to tectonic reconstructions and paleoseismic studies. One way to address this issue is by constraining the timing of fault striations, but this requires a better understanding of the striation formation mechanism and associated mineralization. We present results from a microstructural, geochemical, and geochronological study of calcite precipitates associated with striated fault planes from the Dead Sea fault zone in northern Israel. We recognize four types of coexisting calcite precipitates, including calcite cement in dilation breccia, calcite in striated groove morphology, calcite gouge associated with hydraulic fracturing and pressure solution, and calcite coating of the fault surface.
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Direct dating of brittle fault activity is of fundamental importance to tectonic reconstructions and paleoseismic studies. One way to address this issue is by constraining the timing of fault striations, but this requires a better understanding of the striation formation mechanism and associated mineralization. We present results from a microstructural, geochemical, and geochronological study of calcite precipitates associated with striated fault planes from the Dead Sea fault zone in northern Israel. We recognize four types of coexisting calcite precipitates, including calcite cement in dilation breccia, calcite in striated groove morphology, calcite gouge associated with hydraulic fracturing and pressure solution, and calcite coating of the fault surface. Using U-Th dating of samples from three adjacent fault planes, we delineate four welldefined deformation ages in the period from to 60 ka.

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